Littérature scientifique sur le sujet « Wide Angle Reflection/Refraction »
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Articles de revues sur le sujet "Wide Angle Reflection/Refraction"
Rendleman, C. A., et F. K. Levin. « Reflection maxima for reflections from single interfaces ». GEOPHYSICS 53, no 2 (février 1988) : 271–75. http://dx.doi.org/10.1190/1.1442462.
Texte intégralFilatova, Elena, et Andrey Sokolov. « Effect of reflection and refraction on NEXAFS spectra measured in TEY mode ». Journal of Synchrotron Radiation 25, no 1 (1 janvier 2018) : 232–40. http://dx.doi.org/10.1107/s1600577517016253.
Texte intégralMereu, R. F. « The complexity of the crust from refraction/wide-angle reflection data ». Pure and Applied Geophysics PAGEOPH 132, no 1-2 (1990) : 269–88. http://dx.doi.org/10.1007/bf00874366.
Texte intégralMereu, R. F. « The complexity of the crust and Moho under the southeastern Superior and Grenville provinces of the Canadian Shield from seismic refraction - wide-angle reflection data ». Canadian Journal of Earth Sciences 37, no 2-3 (2 avril 2000) : 439–58. http://dx.doi.org/10.1139/e99-122.
Texte intégralLuetgert, James, et Carol E. Mann. « Avalon terrane in eastern coastal Maine : Seismic refraction-wide-angle reflection data ». Geology 18, no 9 (1990) : 878. http://dx.doi.org/10.1130/0091-7613(1990)018<0878:atiecm>2.3.co;2.
Texte intégralPawlik, G., K. Tarnowski, W. Walasik, A. C. Mitus et I. C. Khoo. « Liquid crystal hyperbolic metamaterial for wide-angle negative–positive refraction and reflection ». Optics Letters 39, no 7 (19 mars 2014) : 1744. http://dx.doi.org/10.1364/ol.39.001744.
Texte intégralMajdański, M. « The uncertainty in layered models from wide-angle seismic data ». GEOPHYSICS 78, no 3 (1 mai 2013) : WB31—WB36. http://dx.doi.org/10.1190/geo2012-0280.1.
Texte intégralNémeth, Balázs, Ron M. Clowes et Zoltan Hajnal. « Lithospheric structure of the Trans-Hudson Orogen from seismic refraction - wide-angle reflection studies ». Canadian Journal of Earth Sciences 42, no 4 (1 avril 2005) : 435–56. http://dx.doi.org/10.1139/e05-032.
Texte intégralRoberts, D. G., A. Ginzberg, K. Nunn et R. McQuillin. « The structure of the Rockall Trough from seismic refraction and wide-angle reflection measurements ». Nature 332, no 6165 (avril 1988) : 632–35. http://dx.doi.org/10.1038/332632a0.
Texte intégralHole, J. A., R. M. Clowes et R. M. Ellis. « Interpretation of three-dimensional seismic refraction data from western Hecate Strait, British Columbia : structure of the crust ». Canadian Journal of Earth Sciences 30, no 7 (1 juillet 1993) : 1440–52. http://dx.doi.org/10.1139/e93-124.
Texte intégralThèses sur le sujet "Wide Angle Reflection/Refraction"
Harsha, Senusi Mohamed. « Interpretation of Southern Georgia coastal plain velocity structure using refraction and wide-angle reflection methods ». Thesis, Georgia Institute of Technology, 1988. http://hdl.handle.net/1853/25886.
Texte intégralHananto, Nugroho. « Architecture and Evolution of North Sumatra Subduction Zone based on long Offset Seismic Reflection and Wide Angle Seismic Refraction / Reflection Data ». Institut de physique du globe (Paris), 2011. http://www.theses.fr/2011GLOB1203.
Texte intégralHughes, Stephen. « Crustal structure of northeastern North America : results from the Ontario-New York-New England seismic refraction/wide-angle reflection experiment ». Thesis, University of Leicester, 1992. http://hdl.handle.net/2381/35043.
Texte intégralMeléndez, i. Catalán Adrià. « Development of a New Parallel Code for 3-D Joint Refraction and Reflection Travel-Time Tomography of Wide-Angle Seismic Data. Synthetic and Real Data Applications to the Study of Subduction Zones ». Doctoral thesis, Universitat de Barcelona, 2014. http://hdl.handle.net/10803/289786.
Texte intégralAquesta tesi està dedicada a la tomografia sísmica. Concretament, he implementat una eina de modelització 3D per a la tomografia conjunta de temps de trajecte de refraccions i reflexions (TOMO3D). La raó darrere d'aquest objectiu és l'evidència de que la informació basada en dades sísmiques 2D no permet copsar la complexitat de gran part dels cossos geològics, i en particular de la zona sismogènica en marges de subducció. El desenvolupament del TOMO3D es basa en el TOMO2D, un codi d'avantguarda per a la tomografia conjunta de refraccions i reflexions en 2D. Els arxius de codi han estat reescrits, redefinint i introduint les funcions necessàries per dur a terme la inversió 3D. Els testos fets amb la versió seqüencial del codi posen de manifest la necessitat de paral·lelització ja que l'increment de la mida dels conjunts de dades així com la modelització de la dimensió espacial afegida fan que les inversions siguin computacionalment exigents. La versió paral·lelitzada del TOMO3D ha sigut aplicada a un cas sintètic complex que simula una zona de subducció. Aquesta primera aplicació 3D serveix per avaluar la correcció de la programació del codi, i com a descripció pas a pas del procediment de modelització. Els resultats demostren la capacitat del codi per recuperar acuradament la distribució de velocitat i la geometria dels dos reflectors. Finalment, el TOMO3D és aplicat a un conjunt 3D de dades de sísmica de gran angle adquirit al marge pacífic d'Equador i Colòmbia per extreure'n un model 3D de la velocitat de les plaques cavalcant i subduïda, que és comparat amb el resultat obtingut amb un codi 3D de tomografia de temps de trajecte de refraccions (FAST). La comparació indica que el TOMO3D és més acurat que el FAST però al mateix temps és computacionalment més exigent. Tot i així, la paral·lelització del TOMO3D permet utilitzar plataformes de supercomputació, a diferència del que passa amb el FAST i la majoria de codis existents.
Brancatelli, Giuseppe. « Analisi di dati acquisiti con OBS ». Doctoral thesis, Università degli studi di Trieste, 2010. http://hdl.handle.net/10077/3458.
Texte intégralGli OBS (Ocean Bottom Seismometer) sono ampiamente utilizzati negli studi sismici crostali attraverso l’utilizzo delle registrazioni di onde rifratte e riflesse a grande offset (Wide Angle Reflection/Refraction, WAR/R). L'analisi di questi dati comporta, solitamente, l'impiego di modellistica diretta e/o inversa al fine di giungere alle velocità dei singoli strati e alle profondità delle interfacce. In questa tesi, invece, si presenta un approccio diverso che prevede: 1) costruzione di modelli di velocità dall’analisi dei segnali rifratti; 2) elaborazione dei dati OBS al fine di ottenere immagini sismiche a riflessione. In particolare, gli OBS e gli scoppi sono stati riportati ad uno stesso datum (superficie del mare), utilizzando il Wave Equation Datuming (WED). Dopo il WED è stato possibile applicare l'elaborazione tipica della sismica a riflessione. I profili OBS analizzati sono stati acquisiti nell'area dell'Arco Ellenico e, i risultati ottenuti, hanno permesso di riconoscere le strutture geologiche principali e i meccanismi dell’evoluzione tettonica. L'utilizzo del WED ha migliorato la risoluzione delle sezioni finali rispetto a quanto ottenibile con le correzioni statiche classiche. Per confronto è stata applicata la metodologia WED anche a dati simici ad alta risoluzione a terra, risolvendo problemi di correzioni statiche e di strutturazioni tettoniche apparenti nell'area della Bassa Pianura Friulana.
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Lester, W. Ryan. « Structure of the Chesapeake Bay Impact Crater from Wide-Angle Seismic Waveform Tomography ». Thesis, Virginia Tech, 2006. http://hdl.handle.net/10919/35090.
Texte intégralMaster of Science
Oueity, Jounada. « Near-vertical and wide-angle seismic reflection studies of the Moho and sub-crustal lithosphere in NW Canada ». Thesis, University of British Columbia, 2010. http://hdl.handle.net/2429/28903.
Texte intégralBiari, Youssef. « Structure profonde de la marge Nord-Ouest Africaine ». Thesis, Brest, 2015. http://www.theses.fr/2015BRES0080/document.
Texte intégralThe NE American margin represents one of the best studied margins in the world, it was the subject of several scientific programs. In comparison, the conjugate NW African margin remains fairly unknown, only two deep seismic cruises were acquired: the SISMAR cruise (2001) offshore the Meseta and the DAKHLA cruise (2002) offshore the Sahara. The deep structure of the Canadian margin is known due to the SMART wide-angle seismic profiles 1, 2 and 3. The first objective of the MIRROR project was to acquire combined wide-angle and deep reflection seismic data offshore a segment conjugate to the SMART-1 profile. The comparison between the homologous segments of these two margins aimed to better understand the opening mechanism of the Central Atlantic Ocean. A comparison between Sismar, Dakhla and Mirror models shows that the continental crust is thicker in the north and thins toward the south. The width of the transition zone is narrower south and Sismar profiles are located on a sedimentary basin placed on a very thinned continental crust. Comparing the Mirror profile with that of the Canadian conjugate margin (Smart 1) shows that the thickness, the structure of the continental crust and the thinning is very similar. However, zones of exhumed and serpentinized mantle were imaged along the Canadian profile that have no conjugate on the African margin. Moreover, the thickness of the oceanic crust is variable with 8 km on the African side and only 3-4 km on the Canadian margin. Several hypotheses have been proposed to explain this difference (a) an age difference between the two types of crust (b) thickening associated with the passage of the Canary hotspot (c) an asymmetric accretion or (d) an accretion at slow to ultra-slow speading centers
Bouyahiaoui, Boualem. « Structure profonde et réactivation de la marge est-algérienne et du bassin adjacent (secteur d'Annaba), contraintes par sismique réflexion multitrace et grand-angle terre-mer ». Thesis, Nice, 2014. http://www.theses.fr/2014NICE4116/document.
Texte intégralIn this study, we determine the deep structure of the eastern Algerian basin and its southern margin in the Annaba region (easternmost Algeria), to better constrain the plate kinematic reconstruction in this region. This study is based on new geophysical data collected during the SPIRAL cruise in 2009 that included a wide-angle, 240-km-long, onshore-offshore seismic profile, multichannel seismic reflection lines, and gravity and magnetic data, which was complemented by the available geophysical data for the study area. The analysis and modeling of the wide-angle seismic data using travel-times and amplitudes, and integrated with the multichannel seismic lines, reveal the detailed structure of an ocean-to-continent transition. In the deep basin, there is an ~5.5-km-thick oceanic crust that is composed of two layers. The upper layer of the crust is defined by a high velocity gradient and P-wave velocities between 4.8 km/s and 6.0 km/s from the top to the bottom. The lower crust is defined by a lower velocity gradient and P-wave velocity between 6.0 km/s and 7.1 km/s. The Poisson ratio in the lower crust deduced from S-wave modeling is 0.28, which indicates that the lower crust is composed mainly of gabbros. Below the continental edge, a typical continental crust with P-wave velocities between 5.2 km/s and 7.0 km/s from the top to the bottom shows a gradual seaward thinning of ~15 km over an ~35-km distance
Laurencin, Muriel. « Etude de la géométrie, de la nature et des déformations de la zone de subduction des Petites Antilles du Nord ». Thesis, Brest, 2017. http://www.theses.fr/2017BRES0096/document.
Texte intégralIn subduction zones, the 3D geometry of the plate interface is one of the key parameters that controls margin tectonic deformation, interplate coupling and seismogenic behavior. The North American plate subducts below the Caribbean plate with a convergence rate of 20 mm/y. The seismic activity is heterogeneous and increases locally under the Virgin Islands platform. The northward increasing convergence obliquity is favorable in partitioning which deformations were not really observed. This PhD confirms that the forearc crust is a crust of oceanic affinity thickened by hotspot magmatism and poorly affected by subduction magmatism. Two structures accommodating the partitioning of the deformation were identified. The Bunce Fault is a 850-kmlength sinistral strike-slip fault extending from Hispaniola to the east of Barbuda decoupling the accretionary prism from the Caribbean substratum. The Anegada Passage, whose extension towards the NE is highlighted, entailed deeply the forearc. The structures are reactivated in sinistral strike-slip faults compatible with the partitioning of the deformation after formation in extension due to the collision of the Bahamas Bank with the northern margin. We image for the first time the characteristics of a slow ridge formation (partly complex core and partly oceanic grain) entering in subduction. It affects the morphology of the accretion prism and probably the seismogenic potential of the subduction interface. We have highlighted a shallower slab which is located under the NE Anegada Passage and where earthquakes and partitioning deformations increase locally. Thus, the shallowing slab might results in a local greater interplate coupling favoring seismic activity and tectonic partitioning beneath the Anegada Passage
Livres sur le sujet "Wide Angle Reflection/Refraction"
J, Moses Michael, et Geological Survey (U.S.), dir. Wide-angle seismic recordings obtained during the tact multichannel reflection profiling in the northern Gulf of Alaska. Menlo Park, Calif : U.S. Dept. of the Interior, U.S. Geological Survey, 1990.
Trouver le texte intégralBrocher, Thomas M. Wide-angle seismic recordings obtained during the tact multichannel reflection profiling in the northern Gulf of Alaska. Menlo Park, Calif : U.S. Dept. of the Interior, U.S. Geological Survey, 1990.
Trouver le texte intégralBrocher, Thomas M. Wide-angle seismic recordings obtained during the tact multichannel reflection profiling in the northern Gulf of Alaska. Menlo Park, Calif : U.S. Dept. of the Interior, U.S. Geological Survey, 1990.
Trouver le texte intégralBrocher, Thomas M. Wide-angle seismic recordings obtained during the tact multichannel reflection profiling in the northern Gulf of Alaska. Menlo Park, Calif : U.S. Dept. of the Interior, U.S. Geological Survey, 1990.
Trouver le texte intégralRiahi, M. Ali. Crustal two- and three-dimensional models of the Gulf of Bothnia area based on wide-angle and normal-incidence seismic data. Uppsala : Acta Universitatis Upsaliensis, 1995.
Trouver le texte intégralJ, Moses Michael, et Geological Survey (U.S.), dir. Onshore-offshore wide-angle seismic recordings of the San Francisco Bay Area Seismic Imaging Experiment (BASIX) : The five-day recorder data. Menlo Park, Calif : U.S. Dept. of the Interior, U.S. Geological Survey, 1993.
Trouver le texte intégralBrocher, Thomas Mark. Onshore-offshore wide-angle seismic recordings of the San Francisco Bay Area Seismic Imaging Experiment (BASIX) : The five-day recorder data. Menlo Park, Calif : U.S. Dept. of the Interior, U.S. Geological Survey, 1993.
Trouver le texte intégralBrocher, Thomas M. Onshore-offshore wide-angle seismic recordings of the San Francisco Bay Area Seismic Imaging Experiment (BASIX) : The five-day recorder data. Menlo Park, Calif : U.S. Dept. of the Interior, U.S. Geological Survey, 1993.
Trouver le texte intégralNovak, Olaf. A wide-angle seismic study of the SE-flank of the Kenya Rift in corporating a multidisciplinary interpretation. Dublin : University College Dublin, 1997.
Trouver le texte intégralBrocher, Thomas Mark. Onshore-offshore wide-angle seismic recordings of the San Francisco Bay Area Seismic Imaging Experiment (BASIX) : Data from the Northern California Seismic Network. Menlo Park, Ca : U.S. Dept. of the Interior, U.S. Geological Survey, 1994.
Trouver le texte intégralChapitres de livres sur le sujet "Wide Angle Reflection/Refraction"
Rumpel, Hanna-Maria, Claus Prodehl, Catherine M. Snelson et G. Randy Keller. « Results of the CD-ROM project seismic refraction/wide-angle reflection experiment : The upper and middle crust ». Dans The Rocky Mountain Region—An Evolving Lithosphere : Tectonics, Geochemistry, and Geophysics, 257–69. Washington, D. C. : American Geophysical Union, 2005. http://dx.doi.org/10.1029/154gm20.
Texte intégralSnelson, Catherine M., G. Randy Keller, Kate C. Miller, Hanna-Maria Rumpel et Claus Prodehl. « Regional crustal structure derived from the CD-ROM 99 seismic refraction/wide-angle reflection profile : The lower crust and upper mantle ». Dans The Rocky Mountain Region—An Evolving Lithosphere : Tectonics, Geochemistry, and Geophysics, 271–91. Washington, D. C. : American Geophysical Union, 2005. http://dx.doi.org/10.1029/154gm21.
Texte intégralEpili, Duryodhan, et Robert F. Mereu. « The GLIMPCE seismic experiment : Onshore refraction and wide-angle reflection observations from a fan line over the Lake Superior Midcontinent Rift System ». Dans Properties and Processes of Earth' Lower Crust, 93–101. Washington, D. C. : American Geophysical Union, 1989. http://dx.doi.org/10.1029/gm051p0093.
Texte intégralGarrett, Steven L. « Reflection, Transmission, and Refraction ». Dans Understanding Acoustics, 513–42. Cham : Springer International Publishing, 2020. http://dx.doi.org/10.1007/978-3-030-44787-8_11.
Texte intégralNeurieder, P. « Seismic Standard Software in Refraction and Wide-Angle Applications ». Dans Joint Interpretation of Geophysical and Geological Data Applied to Lithospheric Studies, 71–91. Dordrecht : Springer Netherlands, 1991. http://dx.doi.org/10.1007/978-94-011-3590-0_5.
Texte intégralBraile, L. W., et C. S. Chiangl. « The continental Mohorovičič Discontinuity : Results from near-vertical and wide-angle seismic reflection studies ». Dans Reflection Seismology : A Global Perspective, 257–72. Washington, D. C. : American Geophysical Union, 1986. http://dx.doi.org/10.1029/gd013p0257.
Texte intégralNowack, Robert L. « Applications of Inverse Methods to the Analysis of Refraction and Wide-Angle Seismic Data ». Dans Inverse Problems in Wave Propagation, 395–417. New York, NY : Springer New York, 1997. http://dx.doi.org/10.1007/978-1-4612-1878-4_20.
Texte intégralMereu, Robert, Dapeng Wang et Oliver Kuhn. « Evidence for an inactive rift in the Precambrian from a wide-angle reflection survey across the Ottawa-Bonnechere graben ». Dans Reflection Seismology : The Continental Crust, 127–34. Washington, D. C. : American Geophysical Union, 1986. http://dx.doi.org/10.1029/gd014p0127.
Texte intégralMereu, Robert. « The Heterogeneity of the Crust and its Effect on Seismic Wide-Angle Reflection Fields ». Dans Heterogeneity in the Crust and Upper Mantle, 257–79. Boston, MA : Springer US, 2003. http://dx.doi.org/10.1007/978-1-4615-0103-9_10.
Texte intégralRokhlin, S. I., T. K. Bolland et L. Adler. « Effects of Reflection and Refraction of Ultrasonic Waves on the Angle Beam Inspection of Anisotropic Composite Material ». Dans Review of Progress in Quantitative Nondestructive Evaluation, 1103–10. Boston, MA : Springer US, 1987. http://dx.doi.org/10.1007/978-1-4613-1893-4_126.
Texte intégralActes de conférences sur le sujet "Wide Angle Reflection/Refraction"
« Workshop 6—Refraction and wide-angle reflections ». Dans 1985 SEG Technical Program Expanded Abstracts. SEG, 1985. http://dx.doi.org/10.1190/1.1892767.
Texte intégralBotelho, Marco A., Irshad R. Mufti et Vicente P. Neto. « Multishot prestack depth migration : An application on wide‐angle reflection and refraction GPR data ». Dans SEG Technical Program Expanded Abstracts 1998. Society of Exploration Geophysicists, 1998. http://dx.doi.org/10.1190/1.1820166.
Texte intégralJiao, Lingxiu, Wooil Moon et W. Kinsner. « Detection of refraction and wide angle reflection signals using the variance fractal dimension trajectory technique ». Dans SEG Technical Program Expanded Abstracts 1997. Society of Exploration Geophysicists, 1997. http://dx.doi.org/10.1190/1.1885646.
Texte intégralJiao, Lingxiu, et Wooil M. Moon. « 3-D seismic modelling using Lithoprobe AGT’92 high resolution seismic wide angle reflection and refraction data in Sudbury, Ontario, Canada ». Dans 6th SAGA Biennial Conference and Exhibition. European Association of Geoscientists & Engineers, 1999. http://dx.doi.org/10.3997/2214-4609-pdb.221.055.
Texte intégralBarr, Sandra, H. Ruth Jackson, Deping Chian, John Shimeld, Chris E. White et Matthew Salisbury. « CONTRASTS IN CRUSTAL CHARACTER BETWEEN MEGUMA AND AVALONIA BASED ON WIDE-ANGLE SEISMIC REFLECTION/REFRACTION PROFILES ALONG THE SCOTIAN MARGIN AND ACROSS NOVA SCOTIA, CANADA ». Dans Northeastern Section - 57th Annual Meeting - 2022. Geological Society of America, 2022. http://dx.doi.org/10.1130/abs/2022ne-374511.
Texte intégralMatsui, Yutaka, et Yukinori Iizuka. « Basic Performance of Normal Incidence Method for Inspection of Middle Zone of Wall Thickness of LSAW Steel Pipes ». Dans 2016 11th International Pipeline Conference. American Society of Mechanical Engineers, 2016. http://dx.doi.org/10.1115/ipc2016-64328.
Texte intégralWadhwa, Abhishek, et Sung-Yong Park. « Optical Analyses of Microfluidic Tunable Liquid Prisms for Enhanced Solar Energy Collection ». Dans ASME 2014 International Mechanical Engineering Congress and Exposition. American Society of Mechanical Engineers, 2014. http://dx.doi.org/10.1115/imece2014-37797.
Texte intégralHadley, G. Ronald. « Comprehensive device simulation via solution of the 2-D Helmholtz equation ». Dans OSA Annual Meeting. Washington, D.C. : Optica Publishing Group, 1992. http://dx.doi.org/10.1364/oam.1992.mw4.
Texte intégralEdgerton, Robert F. « Optical Characterization of TiO2 and SiO2 in Single Films and Double Layer Stacks ». Dans Optical Interference Coatings. Washington, D.C. : Optica Publishing Group, 1992. http://dx.doi.org/10.1364/oic.1992.othd5.
Texte intégralAntonov, Alexander A., et Maxim V. Gorkunov. « Dielectric Fourier Metasurfaces for Wide-Angle Reconfigurable Anomalous Refraction ». Dans Novel Optical Materials and Applications. Washington, D.C. : OSA, 2021. http://dx.doi.org/10.1364/noma.2021.noth2d.3.
Texte intégralRapports d'organisations sur le sujet "Wide Angle Reflection/Refraction"
Riedel, M., M. M. Côté, P. J. Neelands, G. Middleton, G. Standen, R. Iuliucci, M. Ulmi et al. 2012 Haida Gwaii Mw 7.7 earthquake response - ocean bottom seismometer relocation and geophone orientation analysis and quality control of wide-angle P-wave refraction data. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2014. http://dx.doi.org/10.4095/295551.
Texte intégralKeen, C. E. Conversion of seismic-reflection time to depth for the Labrador margin, Davis Strait, and Baffin Bay, offshore northern Canada and Greenland, using sonic logs, checkshot surveys, and wide-angle seismic velocities. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2019. http://dx.doi.org/10.4095/315016.
Texte intégralWilson, D., Michael Shaw, Vladimir Ostashev, Michael Muhlestein, Ross Alter, Michelle Swearingen et Sarah McComas. Numerical modeling of mesoscale infrasound propagation in the Arctic. Engineer Research and Development Center (U.S.), octobre 2022. http://dx.doi.org/10.21079/11681/45788.
Texte intégralKeen, C. E., K. Dickie, L. T. Dafoe, T. Funck, J. K. Welford, S A Dehler, U. Gregersen et K J DesRoches. Rifting and evolution of the Labrador-Baffin Seaway. Natural Resources Canada/CMSS/Information Management, 2022. http://dx.doi.org/10.4095/321854.
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